TY - JOUR
T1 - Microbial competition for phosphorus limits the CO2 response of a mature forest
AU - Jiang, Mingkai
AU - Crous, Kristine Y.
AU - Carrillo, Yolima
AU - Macdonald, Catriona A.
AU - Anderson, Ian C.
AU - Boer, Matthias M.
AU - Farrell, Mark
AU - Gherlenda, Andrew N.
AU - Castañeda-Gómez, Laura
AU - Hasegawa, Shun
AU - Jarosch, Klaus
AU - Milham, Paul J.
AU - Ochoa-Hueso, Rául
AU - Pathare, Varsha
AU - Pihlblad, Johanna
AU - Piñeiro, Juan
AU - Powell, Jeff R.
AU - Power, Sally A.
AU - Reich, Peter B.
AU - Riegler, Markus
AU - Zaehle, Sönke
AU - Smith, Benjamin
AU - Medlyn, Belinda E.
AU - Ellsworth, David S.
N1 - Data archiving: waiting for mail
PY - 2024/6/5
Y1 - 2024/6/5
N2 - The capacity for terrestrial ecosystems to sequester additional carbon (C) with rising CO2 concentrations depends on soil nutrient availability1,2. Previous evidence suggested that mature forests growing on phosphorus (P)-deprived soils had limited capacity to sequester extra biomass under elevated CO2 (refs. 3,4,5,6), but uncertainty about ecosystem P cycling and its CO2 response represents a crucial bottleneck for mechanistic prediction of the land C sink under climate change7. Here, by compiling the first comprehensive P budget for a P-limited mature forest exposed to elevated CO2, we show a high likelihood that P captured by soil microorganisms constrains ecosystem P recycling and availability for plant uptake. Trees used P efficiently, but microbial pre-emption of mineralized soil P seemed to limit the capacity of trees for increased P uptake and assimilation under elevated CO2 and, therefore, their capacity to sequester extra C. Plant strategies to stimulate microbial P cycling and plant P uptake, such as increasing rhizosphere C release to soil, will probably be necessary for P-limited forests to increase C capture into new biomass. Our results identify the key mechanisms by which P availability limits CO2 fertilization of tree growth and will guide the development of Earth system models to predict future long-term C storage.
AB - The capacity for terrestrial ecosystems to sequester additional carbon (C) with rising CO2 concentrations depends on soil nutrient availability1,2. Previous evidence suggested that mature forests growing on phosphorus (P)-deprived soils had limited capacity to sequester extra biomass under elevated CO2 (refs. 3,4,5,6), but uncertainty about ecosystem P cycling and its CO2 response represents a crucial bottleneck for mechanistic prediction of the land C sink under climate change7. Here, by compiling the first comprehensive P budget for a P-limited mature forest exposed to elevated CO2, we show a high likelihood that P captured by soil microorganisms constrains ecosystem P recycling and availability for plant uptake. Trees used P efficiently, but microbial pre-emption of mineralized soil P seemed to limit the capacity of trees for increased P uptake and assimilation under elevated CO2 and, therefore, their capacity to sequester extra C. Plant strategies to stimulate microbial P cycling and plant P uptake, such as increasing rhizosphere C release to soil, will probably be necessary for P-limited forests to increase C capture into new biomass. Our results identify the key mechanisms by which P availability limits CO2 fertilization of tree growth and will guide the development of Earth system models to predict future long-term C storage.
U2 - 10.1038/s41586-024-07491-0
DO - 10.1038/s41586-024-07491-0
M3 - Article
SN - 0028-0836
JO - Nature
JF - Nature
ER -